Digital mapping of buried soil horizons using 2D and pseudo‐3D geoelectrical measurements in a ground moraine landscape

Author(s):  
I. Kroef ◽  
S. Koszinski ◽  
M. Grinat ◽  
M. Meij ◽  
W. Hierold ◽  
...  
2020 ◽  
Author(s):  
Francesca Calitri ◽  
Markus Egli ◽  
Michael Sommer ◽  
Dmitry Tikhomirov ◽  
Marcus Christl

<p><span>In hilly and mountainous landscapes, the bedrock is actively converted to a continuous soil mantle. The bedrock-soil interface lowers spatially at the soil production rate, and the soil acts as a layer removing sediment produced locally and transported from upslope. Forested soils of a hummocky ground moraine landscape in Northern Germany exhibit strongly varying soil thicknesses with very shallow soils on crest positions and buried soils at the footslope. We explored the explanatory power of both <sup>10</sup>Be forms (in situ and meteoric) for forest soils on a hillslope to shed light into the </span><span>complex mass redistribution. </span><span>Our main research questions were: how do meteoric and in-situ <sup>10</sup>Be compare to each other? What do they really indicate in terms of soil processes (erosion, sedimentation, reworking)? </span><span>By using both types of <sup>10</sup>Be, the dynamics of soils and related mass transports should be better traceable</span><span>. Both <sup>10</sup>Be forms were measured along three profiles at different slope positions: Hydro1 (summit), Hydro3 (shoulder), Hydro4 (backslope). Furthermore, a buried horizon was found in the profile Hydro4 at 160 cm depth and <sup>14</sup>C-dated. The distribution pattern of meteoric <sup>10</sup>Be of Hydro4 shows an inverse exponential depth profile, and an almost uniform content of in-situ <sup>10</sup>Be along the profile. Meteoric <sup>10</sup>Be indicates on the one hand that a new soil was put on top of an older, now buried soil. On the other hand, meteoric <sup>10</sup>Be is involved in pedogenetic processes and clearly exhibits clay eluviation in the topsoil and clay illuviation in the subsoil. The uniform content of the in situ <sup>10</sup>Be shows soil mixing that must have occurred during erosion and sedimentation. The<sup>14</sup>C dated buried soil horizon indicates a deposition of eroded soil material about 7 ka BP. Consequently, an increase in the in-situ <sup>10</sup>Be content towards the surface should be expect which however was not the case. The reason for this is so far unknown. Radiocarbon dating and <sup>10</sup>Be data demonstrate that strong events of soil mass redistribution in Melzower Forest are mainly a result of ancient natural events. Further measurements of fallout radionuclides (<sup>239+240</sup>Pu) showed no erosion for the last few decades in the same catchment.</span></p>


Geosciences ◽  
2018 ◽  
Vol 8 (12) ◽  
pp. 492 ◽  
Author(s):  
Marina Lebedeva ◽  
Alexander Makeev ◽  
Alexey Rusakov ◽  
Tatiana Romanis ◽  
Tamara Yanina ◽  
...  

Surface Kastanozem of the Lower Volga area was first studied as a part of the pedocomplex, with the lower part (148–160 cm) formed in Early Khvalynian Chocolate clays (13–15 ka), the middle part (100–148 cm) in a mixed clay-loess sediment sand, and the upper part (0–100 cm) in loess. This resulted from local aeolian transport, with the source material derived from the rewinding of marine sediments. They are enriched in aggregates of Chocolate clays and glauconitic grains of a fine sand-course silt size and have similar contents of clay minerals. The high salinity of similar types evidences marine genesis for both Chocolate clays and source material for loess sediments. Clay fragments of a sand and silt size are responsible for the heavy texture and high gypsum content of loess. The study of soils with the focus on micromorphology and clay mineralogy allows the identification of the complex character of a shift from marine to sub-areal sedimentation. This shift was accompanied by short breaks in sedimentation, allowing the development of synlithogenic soil horizons of Late Khvalynian, after-Khvanynian, and Boreal time. The features of shallowly buried soil horizons confirm increased aridity after the last deglaciation. Surface Calcic Kastanozem is a full Holocene soil reflecting the present environment. However, it is deeply influenced by shallow buried soil horizons and Chocolate clays.


CATENA ◽  
1983 ◽  
Vol 10 (1-2) ◽  
pp. 167-173 ◽  
Author(s):  
J.F. Dormaar ◽  
L.E. Lutwick
Keyword(s):  

1964 ◽  
Vol 15 (1) ◽  
pp. 164-180
Author(s):  
Ekke W. Guenther ◽  
Fritz Tidelski

Abstract. The Murg profile shows a loamy ground moraine as the lowermost Pleistocene layer over gneis. The moraine originated during the furthest thrust of the Alpine glaciers in the direction of the Black Forest, and has been placed since 1909 (according to the work of Penck and Brückner) in the Riss glacial stage. Overlying the moraine are pollenbearing peat bog and pond deposits. The pollen indicate, in the deepest layers, a plant community that might still be possible under present climatic conditions. In the higher layers, the trees having affinities to warm conditions disappear. The composite diagram (pollen spectrum) indicates the end phase of an interglacial stage. Over these sediments lie 6—10 m of loess and loess-loam deposits. A thick loam layer, averaging 2.50 m in width, which contains more or less distinct soil horizons, lies between aeolian loess, which always represents a cold period. It can thus be proved that at least a part of these substrata originated in place. Since this loam horizon also represents a warm phase, the deposits of two warm periods overlie the Riss moraine in the Murg profile. Remains of elephants, giant stags, and bison permit comparison of the Murg stratigraphic sequence with a portion of the profile at Achenheim near Strassburg. Hereby is shown that merely the warm period, between the moraine formation and the lowest loess at Murg, can correspond to layers at Achenheim which have yielded the last ancient elephant (Palaeoloxodon antiquus Falc.). These are approximately of the same age as the travertine at Ehringsdorf The pollen-bearing sectionat Murg might then probably be included in the time of formation of the upper travertine at Ehringsdorf.


2016 ◽  
Vol 82 ◽  
pp. 161-191 ◽  
Author(s):  
Jonathan Tabor ◽  
Lawrence Billington ◽  
Frances Healy ◽  
Mark Knight

This paper presents the results of an excavation at North Fen, Sutton Gault, Cambridgeshire, which revealed evidence of Early Neolithic occupation comprising some 48 pits together with twoin situartefact scatters preserved within buried soil horizons. Largely as a result of the spatial separation between scatters and pit sites/clusters, it has been possible to identify a series of ‘sites’, which appear to represent temporally discrete episodes of activity ranging from task-specific ‘visits’ to relatively long-lived occupation. Through analysis of pottery and flint assemblages an attempt is made to characterise each individual site in terms of the types of activities undertaken there and to consider their scale and duration. Set within a landscape that has seen extensive archaeological investigation over the past 30 years the excavation also provides an excellent opportunity to explore how these sites relate to activity in the wider locale and to what extent it is possible to characterise Early Neolithic occupation at a landscape scale.


2007 ◽  
Vol 40 (3) ◽  
pp. 239-248 ◽  
Author(s):  
Mark R. Goulden ◽  
David J. Sauchyn

ABSTRACTThe topography of the west block of the Cypress Hills indicates that fluvial dissection of the plateaux and subsequent rotational landsliding of valley sides have been the dominant Quaternary geomorphic processes. This paper presents a preliminary chronology of rotational landslides based on the relative ages of 17 landslides and on 3 absolute dates. Four indices of relative age were used: organic content in Ah and B soil horizons, the size and coverage of lichens and weathering rind thickness on boulders exposed by landsliding, and the concavity and gradient of gullies in landslide debris, One landslide occurred in 1965. Organic materials collected from buried soil horizons beneath depressions on 3 other landslides were radiocarbon dated at 1235 ± 105, 1635 ± 105 and 7259 ± 165 yrs. BP. Microscopic analysis of the organic material revealed that the oldest sample was contaminated with older carbon. Cluster analysis of the relative age data in conjunction with 3 acceptable absolute dates suggests that the landslides under study have occurred during late Holocene time.


2017 ◽  
Vol 11 (1) ◽  
pp. 126-143
Author(s):  
Ocean Howell

American urban historians have begun to understand that digital mapping provides a potentially powerful tool to describe political power. There are now important projects that map change in the American city along a number of dimensions, including zoning, suburbanization, commercial development, transportation infrastructure, and especially segregation. Most projects use their visual sources to illustrate the material consequences of the policies of powerful agencies and dominant planning ‘regimes.’ As useful as these projects are, they often inadvertently imbue their visualizations with an aura of inevitability, and thereby present political power as a kind of static substance–possess this and you can remake the city to serve your interests. A new project called ‘Imagined San Francisco’ is motivated by a desire to expand upon this approach, treating visual material not only to illustrate outcomes, but also to interrogate historical processes, and using maps, plans, drawings, and photographs not only to show what did happen, but also what might have happened. By enabling users to layer a series of historical urban plans–with a special emphasis on unrealized plans–‘Imagined San Francisco’ presents the city not only as a series of material changes, but also as a contingent process and a battleground for political power.


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